Groundwater impact assessment of Lake Czorsztyn after 25 years of its operation [PDF]
Archives of Environmental Protection, 2022 Artificial water reservoirs pose impact on the natural environment. Impact of the artificial Czorsztyn Lake on groundwater and land management is assessed.
Włodzimierz Humnicki +5 more
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Basin Research, Volume 34, Issue 5, Page 1507-1535, October 2022., 2022 Mechanical accumulations of thin Bositra shells form mounds, with complex internal geometries (yellow dots), on the flat top of a drowned carbonate platform, lending an antiformal geometry to their Kimmeridgian–Tithonian drape (above dashed blue line).
Massimo Santantonio, Cristina Muraro
wiley +1 more source
Gravity measurements in the Pieniny Klippen Belt (Western Slovakia) [PDF]
Geology, Geophysics & Environment, 2015 1 Slovak Academy of Sciences, Geophysical Insitute; Dubravska cesta 9, 845 04 Bratislava, Slovakia; e-mail: geofjabu@savba.sk 2 GEOFOS, s.r.o.; Veľký diel 3323, 010 08 Žilina, Slovakia 3 Comenius University, Faculty of Natural Sciences, Department of Applied and Environmental Geophysics; Mlynska dolina, 842 15 Bratislava 4, Slovakia 4 Comenius ...
Jana Bucová +3 more
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Resolving the Middle Jurassic dinoflagellate radiation: The palynology of the Bajocian of Swabia, southwest Germany [PDF]
, 2017 Dinoflagellates underwent a major radiation during the Bajocian (Middle Jurassic, ~ 170–168 Ma). The group originated in the Middle Triassic and dinoflagellate cysts were relatively low in diversity until the Bajocian, when over 100 species appeared. The
Franz, M, Riding, JB, Wiggan, NJ
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Geological structure and evolution of the Pieniny Klippen Belt to the east of the Dunajec River : a new approach (Western Outer Carpathians, Poland) [PDF]
, 2014 The area studied, known as the Małe (Little) Pieniny Mts., belongs to the Pieniny Klippen Belt (PKB), a suture zone that separates the Central Carpathians from the Outer Carpathian accretionary wedge. Along its northern boundary the PKB is separated from
Oszczypko, Nestor +1 more
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Volumina Jurassica, 2021 The Czertezik Succession of the Pieniny Klippen Belt in Poland is assigned herein to its type area of occurrence – the main Pieniny Range, between Zamkowa Góra and Czertezik mounts.
A. Wierzbowski +3 more
semanticscholar +1 more source
Trace element geochemistry of the Early to Late Cretaceous deposits of the Grajcarek thrust-sheets : a palaeoenvironmental approach (Małe Pieniny Mts., Pieniny Klippen Belt, Poland) [PDF]
, 2012 The chemical composition of the Cretaceous deposits of the Grajcarek thrust-sheets (Pieniny Klippen Belt, Poland) has been investigated to provide information on palaeoenvironment and provenance of pelagic and turbiditic particles.
Oszczypko, Nestor +1 more
core +1 more source
Early Cretaceous intra-plate volcanism in the Pieniny Klippen Belt : a case study of the Velykyi Kamenets'/Vilkhivchyk (Ukraine) and Biała Woda (Poland) sections [PDF]
, 2012 The geological position and geochemistry of the basaltic sill and tuffs occurring within the Berriasian-?Albian pelagic limestones of the Czorsztyn Succession are described.
Krobicki, Michał +2 more
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Геофизический журнал, 2023 Transcarpathian depression (TD) is located in the junction zone of the eastern margin of ALCAPA terrain and the northern part of Tisza-Dacia one, buried under thick Neogene molasses. The Earth’s crust structure of the TD is not clearly understood. The
A. Murovskay +4 more
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